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Kaurilands
Kaurilands is a suburb of West Auckland, which is under the local governance of Auckland Council. The area was subdivided and developed in the 1920s. Geography Kaurilands is located in the Waitākere Ranges foothills north of Titirangi, in the upper catchment of the Waikumete Stream, which flows north through the suburb. Kaurlands forms a part of the Waitematā-Waitākere foothills ecological zone. Sheltered from the Tasman Sea by the Waitākere Ranges, the area was traditionally dominated by forests of kauri, ''Phyllocladus trichomanoides'' (tānekaha or celery pine) and rimu, with abundant nīkau palm and silver fern. The soils are a mix of Miocene Waitākere volcanic soil and Waitemata Group sedimentary rock. History The area is within the traditional rohe of Te Kawerau ā Maki, an iwi that traces their ancestry to some of the earliest inhabitants of the Auckland Region. West Auckland was known as Hikurangi, and the upper catchments of Te Wai-o-Pareira / Henderson Creek ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Konini
Konini is a suburb in the West Auckland, New Zealand, under the local governance of Auckland Council. Kōnini is the Māori language name for the fruit of the tree fuchsia. Geography Konini is enclosed in lush bush at the western ends and tranquil suburban streets to the east. Konini Road is a long bending street that moves from the suburb of Glen Eden to the Waitākere Ranges and native rain forest. Konini forms a part of the Waitematā-Waitākere foothills ecological zone. Sheltered from the Tasman Sea by the Waitākere Ranges, the area was traditionally dominated by forests of kauri, ''Phyllocladus trichomanoides'' (tānekaha or celery pine) and rimu, with abundant nīkau palm and silver fern. The soils are a mix of Miocene Waitākere volcanic soil and Waitemata Group sedimentary rock. History The area is within the traditional rohe of Te Kawerau ā Maki, an iwi that traces their ancestry to some of the earliest inhabitants of the Auckland Region. West Auckland was ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glen Eden, New Zealand
Glen Eden is a suburb of West Auckland, New Zealand, located at the foothills of Waitākere Ranges. Originally known as Waikumete, the suburb gained the name Glen Eden in 1921. The suburb is in the Waitākere Ward, one of the thirteen administrative areas of Auckland governed by Auckland Council. Originally part of the rohe of Te Kawerau ā Maki, the area developed into orchards during the Colonial era of New Zealand. The Glen Eden railway station opened in 1880, linking the area to central Auckland along the Western Line, and leading to the development of the Waikumete Cemetery. Suburban housing was built in the area in the 1950s and 1960s. Geography The Glen Eden area is located at the foothills of Waitākere Ranges, north of Titirangi. The Waikumete Stream flows north from Titirangi, forming a valley in the centre of the suburb. Glen Eden forms a part of the Waitematā-Waitākere foothills ecological zone. Sheltered from the Tasman Sea by the Waitākere Ranges, the are ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Waikumete Stream
The Waikumete Stream is a stream of the Auckland Region of New Zealand's North Island. It flows north from its sources in Titirangi, before joining the Oratia Stream. Both bodies are tributaries of Te Wai-o-Pareira / Henderson Creek, which flows into the western Waitematā Harbour. The stream passes through the suburbs of Titirangi, Kaurilands, Glen Eden and Sunnyvale, and since the mid-2000s has been forested with native flora. Description The stream begins north of Titirangi township, flowing north through the suburbs of Kaurilands and Glen Eden. At Glen Eden, the stream changes course, flowing north-west towards Parrs Park. The stream finishes its course at Millbrook Esplanade in the suburb of Sunnyvale, where it flows into the Oratia Stream. The stream has one tributary, the Hibernia Stream, which flows parallel to the Waikumete Stream to the west, flowing through Wirihana Park and Kowhai Reserve, meeting the Waikumete Stream at Ceramco Park. The stream is a habitat for ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Waitakere City Council
Waitākere City was a territorial authority in West Auckland, New Zealand; it was governed by the Waitākere City Council from 1989 to 2010. It was New Zealand's fifth-largest city, with an annual growth of about 2%. In 2010 the council was amalgamated with the other authorities of the Auckland Region to form the current Auckland Council. The name "Waitākere" comes from the Waitākere River in the Waitākere Ranges. History Before being settled by Europeans, the Māori iwi Te Kawerau a Maki and Ngāti Whātua had already settled in the Waitakere area. In the 1830s, European settlers started to arrive, concentrating on timber milling, kauri gum digging and flax milling, with brickworks and pottery industries following later. In the 20th century, industry and service trades started to grow, with population taking off after World War II, partly due to improved transport links with Auckland City, such as the Northwestern Motorway, whose first section opened in 1952. Subu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Te Kawerau ā Maki
Te Kawerau ā Maki, Te Kawerau a Maki, or Te Kawerau-a-Maki is a Māori ''iwi'' (tribe) of the Auckland Region of New Zealand. It had 251 registered adult members as of June 2017. Auckland Council gave it land for a marae at Te Henga (Bethells Beach) in 2018; it has no ''wharenui'' (meeting house) yet. History Te Kawerau ā Maki are the descendants of the ''rangatira'' (chief) Maki and his wife Rotu, who migrated with their family and followers from Kawhia to Tāmaki Makaurau (Auckland) in the early 1600s. Te Kawerau trace their ancestry from a number of Māori migration canoes, particularly the Tainui, but also Aotea, Tokomaru, Kahuitara and Kurahaupō. Tainui ancestors including Hoturoa and the tohunga Rakataura (Hape) are particularly important in Te Kawerau whakapapa, as is the ancient turehu ancestor and tohunga Tiriwa. Maki and his people were related to a number of groups who had occupied the Auckland region since the fourteenth century, including the Tainui ''hapū'' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geology Of The Auckland Region
The Auckland Region of New Zealand is built on a basement of greywacke rocks that form many of the islands in the Hauraki Gulf, the Hunua Ranges, and land south of Port Waikato. The Waitākere Ranges in the west are the remains of a large andesitic volcano, and Great Barrier Island was formed by the northern end of the Coromandel Volcanic Zone. The Auckland isthmus and North Shore are composed of Waitemata sandstone and mudstone, and portions of the Northland Allochthon extend as far south as Albany. Little Barrier Island was formed by a relatively isolated andesitic volcano, active around 1 to 3 million years ago. The Manukau and South Kaipara Harbours are protected by the recent sand dune deposits of the Awhitu and South Kaipara Peninsulas. Recent basaltic volcanic activity has produced many volcanic cones throughout the Auckland Region, including the iconic Rangitoto Island. Basement rocks As with most of New Zealand, the basement rocks of the Auckland Region are composed o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Waitemata Group
The Waitemata Group is an Early Miocene geologic group that is exposed in and around the Auckland Region of New Zealand, between the Whangarei Harbour in the North and the Raglan Harbour in the South. The Group is predominantly composed of deep water sandstone and mudstone (flysch). The sandstone dominated units form the cliffs around the Waitemata Harbour and rare more resistant conglomerates underlie some of Auckland's prominent ridges. Sub-units and deposition The Waitemata Group was deposited within fault controlled basins. These were bounded to the North and South by up faulted Mesozoic basement sedimentary rocks and volcanic rocks to the East and West. The sedimentary source for the Group's sandstone is a mix of these basement sediments of the Waipapa Terrane and the mostly intermediate volcanic rocks. The maximum water depth of the Waitemata Group basin was 2,000 m. The basal strata (Kawau Subgroup) are from the early Miocene ( Otaian) and range in thickness from 10 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rohe
The Māori people of New Zealand use the word ''rohe'' to describe the territory or boundaries of ''iwi'' (tribes), although some divide their rohe into several ''takiwā''. The areas shown on the map (right) are indicative only, and some iwi areas may overlap. The term ''rohe'' also combines with other words to form more modern terms. These include ''rohe pōti'', meaning an electoral district or constituency, ''rohe wā'', meaning time zone, and ''whatunga rohe paetata'', meaning a local area network. The term ''rohe'' on its own has also been adopted to mean an internet domain. The term is also used for the mission districts (''rohe mihana'') of Te Pīhopatanga o Aotearoa, the Māori Anglican Church in Aotearoa/New Zealand. See also * List of Māori iwi This is a list of iwi (New Zealand Māori tribes). List of iwi This list includes groups recognised as iwi (tribes) in certain contexts. Many are also hapū (sub-tribes) of larger iwi. Moriori are included on this list. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Auckland
Auckland (pronounced ) ( mi, Tāmaki Makaurau) is a large metropolitan city in the North Island of New Zealand. The List of New Zealand urban areas by population, most populous urban area in the country and the List of cities in Oceania by population, fifth largest city in Oceania, Auckland has an urban population of about It is located in the greater Auckland Region—the area governed by Auckland Council—which includes outlying rural areas and the islands of the Hauraki Gulf, and which has a total population of . While European New Zealanders, Europeans continue to make up the plurality of Auckland's population, the city became multicultural and Cosmopolitanism, cosmopolitan in the late-20th century, with Asian New Zealanders, Asians accounting for 31% of the city's population in 2018. Auckland has the fourth largest Foreign born, foreign-born population in the world, with 39% of its residents born overseas. With its large population of Pasifika New Zealanders, the city is ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Auckland Region
Auckland () is one of the sixteen regions of New Zealand, which takes its name from the eponymous urban area. The region encompasses the Auckland Metropolitan Area, smaller towns, rural areas, and the islands of the Hauraki Gulf. Containing percent of the nation's residents, it has by far the largest population and economy of any region of New Zealand, but the second-smallest land area. On 1 November 2010, the Auckland region became a unitary authority administered by the Auckland Council, replacing the previous regional council and seven local councils. In the process, an area in its southeastern corner was transferred to the neighbouring Waikato region. Geography On the mainland, the region extends from the mouth of the Kaipara Harbour in the north across the southern stretches of the Northland Peninsula, through the Waitākere Ranges and the isthmus of Auckland and across the low-lying land surrounding the Manukau Harbour, ending within a few kilometres of the mouth o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Silver Fern
''Alsophila dealbata'', synonym ''Cyathea dealbata'', commonly known as the silver fern or silver tree-fern, or as ponga or punga (from Māori or ),The Māori word , pronounced , has been borrowed into New Zealand English as a generic term for tree ferns. It is also used to refer to tree fern logs when used for landscaping purposes. English speakers generally pronounce the word . is a species of medium-sized tree fern, endemic to New Zealand. The fern is usually recognisable by the silver-white colour of the under-surface of mature fronds. It is a symbol commonly associated with the country both overseas and by New Zealanders themselves. Description This fern is known to grow to heights of or more (though it occasionally takes a rare creeping form). The crown is dense, and mature fronds tend to be about long and have a silver-white colouration on the undersides. This distinctive silver colouration has made them useful for laying along tracks for night walking. The scales ar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Te Wai-o-Pareira / Henderson Creek
The Te Wai-o-Pareira / Henderson Creek is an estuarine river of the Auckland Region of New Zealand's North Island. It flows north from its sources in the Henderson Valley and Titirangi, before reaching the western Waitematā Harbour. Geography The section of the creek known as Te Wai-o-Pareira / Henderson Creek begins at the point when the Opanuku Stream and Oratia Stream intersect at Henderson; where tidal estuarine water from the Waitematā Harbour begins. The creek joins the Mānutewhau Creek at the western edges of the Waitematā Harbour. The south-western arm of the creek where the Momutu and Paremuka streams confluence is known locally as Huruhuru Creek, and traditionally by the name Wai Huruhuru Manawa. Tributaries of Te Wai-o-Pareira / Henderson Creek include the Momutu Stream, Rarawaru Stream, Paremuka Stream, Ōpanuku Stream, Oratia Stream and the Waikumete Stream. History The creek was known by Te Kawerau ā Maki and other Tāmaki Māori as Waipareira or Te W ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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